吉林大学学报(地球科学版)
吉林大學學報(地毬科學版)
길림대학학보(지구과학판)
JOURNAL OF JILIN UNIVERSITY(EARTH SCIENCE EDITION)
2014年
5期
1432-1440
,共9页
尤丽%张迎朝%李才%张哨楠%招湛杰
尤麗%張迎朝%李纔%張哨楠%招湛傑
우려%장영조%리재%장초남%초담걸
“甜点”%低渗储层%沉积相%成岩相%储集性%珠海组%珠江口盆地
“甜點”%低滲儲層%沉積相%成巖相%儲集性%珠海組%珠江口盆地
“첨점”%저삼저층%침적상%성암상%저집성%주해조%주강구분지
“sweet spots”%low permeability reservoir%sedimengtary facies%diagenesis facies%reservoir quality%Zhuhai Formation%Pearl River mouth basin
文昌9区位于珠江口盆地文昌 A 凹陷六号断裂珠三南断裂带之间。古近系珠海组是主要储集层系,埋深基本大于3 km,为扇三角洲前缘潮坪相沉积储层,储层物性以低渗特征为主,局部发育中渗。为扩大勘探油气储量和后期合理有效开发,“甜点”储层寻找至关重要,笔者通过常规物性、测井解释、岩石薄片分析、二维核磁共振等,认识成岩相展布与储集层厚度、物性分布,综合沉积作用、成岩作用等,精细剖析珠海组低渗成因及储集厚度与物性差异发育的主控因素。研究表明:珠海组低渗特征形成的主要原因是压实作用,水下分流河道、潮道和砂坪微相为最有利储集相带,其次为混合坪,二者均可能形成“甜点”储层;压实程度偏弱、粒度较粗、溶蚀较强或绿泥石包壳发育区为潜在的“甜点”储层发育区,可确定六号断裂珠三南断裂带之间发育“甜点”储层;六号断裂带相近埋深,六号断裂带附近区域较远离区域更有利于“甜点”储层发育。
文昌9區位于珠江口盆地文昌 A 凹陷六號斷裂珠三南斷裂帶之間。古近繫珠海組是主要儲集層繫,埋深基本大于3 km,為扇三角洲前緣潮坪相沉積儲層,儲層物性以低滲特徵為主,跼部髮育中滲。為擴大勘探油氣儲量和後期閤理有效開髮,“甜點”儲層尋找至關重要,筆者通過常規物性、測井解釋、巖石薄片分析、二維覈磁共振等,認識成巖相展佈與儲集層厚度、物性分佈,綜閤沉積作用、成巖作用等,精細剖析珠海組低滲成因及儲集厚度與物性差異髮育的主控因素。研究錶明:珠海組低滲特徵形成的主要原因是壓實作用,水下分流河道、潮道和砂坪微相為最有利儲集相帶,其次為混閤坪,二者均可能形成“甜點”儲層;壓實程度偏弱、粒度較粗、溶蝕較彊或綠泥石包殼髮育區為潛在的“甜點”儲層髮育區,可確定六號斷裂珠三南斷裂帶之間髮育“甜點”儲層;六號斷裂帶相近埋深,六號斷裂帶附近區域較遠離區域更有利于“甜點”儲層髮育。
문창9구위우주강구분지문창 A 요함륙호단렬주삼남단렬대지간。고근계주해조시주요저집층계,매심기본대우3 km,위선삼각주전연조평상침적저층,저층물성이저삼특정위주,국부발육중삼。위확대감탐유기저량화후기합리유효개발,“첨점”저층심조지관중요,필자통과상규물성、측정해석、암석박편분석、이유핵자공진등,인식성암상전포여저집층후도、물성분포,종합침적작용、성암작용등,정세부석주해조저삼성인급저집후도여물성차이발육적주공인소。연구표명:주해조저삼특정형성적주요원인시압실작용,수하분류하도、조도화사평미상위최유리저집상대,기차위혼합평,이자균가능형성“첨점”저층;압실정도편약、립도교조、용식교강혹록니석포각발육구위잠재적“첨점”저층발육구,가학정륙호단렬주삼남단렬대지간발육“첨점”저층;륙호단렬대상근매심,륙호단렬대부근구역교원리구역경유리우“첨점”저층발육。
Zhuhai Formation is the major reservoir in ,Wenchang 9 area between the No.6 Fault and the South Fault of Wenchang A depression,which deeply buried over 3 km.It is the rontal subfacies of fan delta.The reservoir properties are low permeability mainly.In order to expanding the prospecting for oil and gas reserves and later the reasonable and effective development,diagenetic facies and the distribution of reservoir thickness and physical properties are recognized by normal physical characteristics,logging interpretatio,analysis of rock thin and two dimensional nuclear magnetic resonance.The reasons of low permeability formation and factors of reservoir thickness and physics quality are analysed finly from sedimentary facies and diagenesis.It is determined that compaction is the main reseron to low permeability.The most favorable Sedimentary facies are underwater distributary channel,tidal channel,sand flat,the second is the mixed flat.All of them can form “sweet spots”reservoir.Less compaction, coarse grain size,the dissolution stronger intensity or chlorite grain-coatings are the areas of “sweet spots”reservoir.The area between the fault zone 6 to the South fault zone of weaker compaction is “sweet spots”reservoir zone.The zones near the fault are more favorable to sweet spots than the zones further away from the sixth fault with similar depth.